...
Internally, Source partitions the link into ndiv divisions (where ndiv is the lag measured in number of model timesteps). Water moves progressively through the link, one division at a time, without attenuation and ignoring any loss and gain fluxes and any dead storage, as follows:
...
Storage Routing links model the storage and movement of water through a length of river using a hydrologic routing method. Storage Routing links They can model represent the travel time of water through a reach, the attenuation of flow rates that can occur due to channel shape and roughness and reach processes (such as lateral fluxes). Reach processes include such things as . Examples of lateral fluxes include net evaporation from the water surface and exchanges between groundwater and surface water.
...
- linear Muskingum routing,
- non-linear Muskingum routing (using a power function),
- variable parameter Muskingum routing
See the Link storage routing - SRG for a detailed description of storage routing.
Storage Routing links can also be configured to represent lag lagged flow , without attenuation (equivalent to a Lagged Flow link, ) but with the capacity to include lateral fluxes, see /wiki/spaces/SD540/pages/255100492.For detailed information, see Link storage routing - SRG. . See the Links user guide for how to configure the Storage Routing link to achieve this, and the Storage Routing Link SRG for information on the solution procedure.